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There are several ways to display the Assets panel. Select the Show Assets button from the Launcher or choose Window Assets. You can also use the keyboard shortcut, F11. Once opened, you ll see that the Assets panel is divided into two areas, a preview and a listing. Images and multimedia are shown as a proportionate thumbnail; Flash, Shockwave, and Movie category previews can be played by selecting the Play button that appears in the preview area when a file is selected. Dreamweaver keeps track of the assets in a site through the use of the site cache, which is enabled when the site is defined. When you open a page in a site and display the Assets panel, the site cache is read and all the available resources are listed. When you add an asset, such as an image or new background color, it appears in the Assets panel automatically the next time a page from the site is opened. You can hasten the process and manually refresh the site cache by selecting the Refresh Site List button on the bottom of the Assets panel. The same procedure holds true for assets removed from your pages.

and hinting as to when garbage collection should occur (by using Systemgc), the only real concrete influence that the programmer has is over the number of allocations Allocate objects less often and allocate smaller objects in order to reduce garbage collection frequency In particular, avoid garbage collector thrashing, which means continuously allocating small objects (such as event objects) Reuse existing objects whenever possible, and refer to the programming strategies discussed in the next chapter The Class Loader A virtual machine needs a way to locate the classes that it needs This task belongs to the class loader The class loader is perhaps the simplest part of the execution engine, but it has an important part to play Its job is to find a class and load it into memory for use by the virtual machine There are two kinds of class loaders.

common scenario in the early days of Java. Nowadays, it is more common to package multiple class files into a single, compressed Java Archive (JAR) file for a variety of reasons. To the VM, however, the class files are still separate entities and are always treated individually. Portability is a key feature of the classfile format. You can take a class file compiled on a particular architecture and move it to another machine without worrying about differences in byte order or character encodings. The JVMS takes care of these and other potential road blocks. For example, strings are stored in UTF-8 format, which is a multi-byte encoding of Unicode, while individual data values that are larger than a single byte are always stored in big-endian (high bytes first) format. Class files are not compact because they store a lot of symbolic information: the name of the class, the names (including the parameter and return types) of methods, field names, the names of other classes and methods referenced by the class, and so on. Some of this information is optional and can be stripped out (debugging information, for example). But most of it is necessary because Java uses symbolic name resolution at run time in order to find classes, methods, and fields. Consider, for example, a simple class with no fields or methods apart from the automatically generated constructor:

over 10 km farther south (Fig 89a) The current smooth shape of the releasing bends formed later, after unconformity DB3, as subsequent strike-slip motion formed faults that joined across the gap between the stepovers (Fig 810a,b) In contrast to the extension that characterizes the northern Dagg Basin, the southern end of the basin shows evidence of reverse faulting and uplift A combination of shortening and strike-slip faulting associated with a restraining bend in this region formed the Dagg Ridge, which has been squeezed upward between the main trace of the Alpine Fault on the west and a curved oblique-slip fault beneath its eastern margin (Fig 89c) South of the ridge, the Breaksea Basin preserves features that indicates it was once continuous with the Dagg Basin, suggesting that the reverse faulting occurred after the pull apart had formed (Barnes et al, 2005).